| PublicID | 2019p582404 |
| UTC Time | 2019-08-04T11:44:18Z |
| Latitude | -49.46 (± 6.2 km) |
| Longitude | 164.53 (± 5.6 km) |
| Depth | 12 km (± 0 km) |
| Depth Type | operator assigned |
| Earth Model | iasp91 |
| Used Phase Count | 40 |
| Used Station Count | 23 |
| Standard Error | 1.75 (s) |
| Azimuthal Gap | 220.34 (degrees) |
| Minimum Distance | 3.50 (degrees) |
| Type | Magnitude | Station Count |
| Preferred (mB) | 6.2 (± 0.2) | |
| M | 6.3 | 11 |
| Mw(mB) | 5.9 (± 0.4) | 6 |
| mB | 6.2 (± 0.2) | 6 |
| ML | 6.7 (± 0.2) | 11 |
| MLv | 6.6 (± 0.2) | 11 |
GeoNet combines magnitudes into a summary magnitude, M, which consists of a weighted average of the individual magnitudes and attempts to be a best possible compromise between all magnitudes for a range of earthquake sizes.
Summary magnitude for GeoNet is then defined as:
M = (2 * MLv + (0.4 * number_of stations(Mw(mB)) - 1) * Mw(mB)) / (2 + (0.4 * number_of_stations(Mw(mB)) - 1))
Where MLv is local magnitude calculated on the vertical component and Mw(mB) is a Mw estimation based of mB by Bormann and Saul (2008).
Map showing stations with picks used to locate the earthquake. Stations with picks that have a zero weight in the solution are shown as small grey circles. Those with a higher weight are shown as larger circles. The quake is shown by the largest circle.